Age of the Marwar Supergroup,NW India:A note on the U–Pb geochronology of Jodhpur Group felsic volcanics |
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作者姓名: | Huiru Xu Joseph G.Meert Manoj K.Pandit |
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作者单位: | Hubei Subsurface Multi-scale Imaging Key Laboratory;Department of Earth and Planetary Sciences;Department of Geology |
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基金项目: | JGM by the US National Science Foundation Grant EAR09-10888;HRX by the National Natural Science Foundation of China Grant 41974078。 |
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摘 要: | The Marwar Supergroup(NW Peninsular India)is thought to be of Ediacaran-Cambrian age,based on previous paleontological and geochronological studies.However,direct constraints on the onset of sedimentation within the Marwar basin are still scarce.In this study,we report U–Pb zircon,LA-ICP-MS,and SIMS ages from the Chhoti Khatu felsic volcanic rocks,interlayered with the Jodhpur Group sandstones(Lower Marwar Supergroup).The cathodoluminescence images of the zircons indicate complex morphologies,and core-rim textures coupled with the wide range of ages indicate that they are likely inherited or in the case of thin poorly indurated ash-beds,detrital in origin.The age spectra of 68 zircon analyses from our sampling display a dominant 800–900 Ma age peak corresponding to the age of basement"Erinpura granite"rocks in the region.The youngest inherited zircon from a felsic ash layer yielded a U–Pb age of651 Ma±18 Ma that,together with previous studies and paleontological evidence,indicates a postCryogenian age for the initiation of Marwar sedimentation following a~125 Ma hiatus between the end of Malani magmatism and Marwar deposition.
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关 键 词: | Marwar Supergroup Sedimentation age Zircon U-Pb dating Chhoti Khatu felsic volcanics |
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